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新疆库鲁克塔格兴地Ⅱ号岩体是一个深源岩浆经多次分异、多期侵入形成的基性-超基性杂岩体.岩体成矿背景条件、岩石化学及岩体矿化特征均显示,该杂岩体内可能赋存有大中型铜镍硫化物矿床.文章通过对成矿背景条件、岩石特征及矿化特征的分析,对该杂岩体的铜镍含矿性做出初步评价.
The No.2 rock mass of the Kluketaghing Hind area in Xinjiang is a basic-ultramafic complex formed by multiple differentiation and multi-stage intrusions of deep-source magmatism. The metallogenetic background conditions, rock chemistry and rock mass Mineralization features show that the complex may have large and medium Cu-Ni sulfide deposits in the body.Through the analysis of metallogenic background, rock characteristics and mineralization characteristics, Make a preliminary evaluation of sex.